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In this paper, characterization of the mortars of different constructive elements in Roman Temple of Diana for its conservation is presented. Mortar samples collected from different parts of the Temple were characterized by means of polarized optical microscopy (POM), X-ray diffraction (XRD), thermal analysis (TGA-DSC) and X-ray fluorescence (XRF).

The optical microscopy results revealed that the mortars are composed of lime binder and quartz, feldspar and biotite grains together with granitic and metamorphic rock fragments as aggregates. XRD analysis supports the microscopic observations and adds the information of the presence of actinolite in the aggregates. XRD analysis further indicates the same origin of the granitic and metamorphic rocks from the surroundings and reveals an absence of biotite in the flooring mortar and only a trace of quartz in the masonry mortar of criptoporticus. According to results of TGA-DSC and XRF analyses, mortars were used in the channel in front of the Temple, the foundation of granite ashlar, and the inner wall of criptoporticus has higher hydraulic character.